. Bulletin of the Geological Society of America. Geology. RELATIONS OF BATITOLTTHIC AREAS 339 The batholxths and the Kruger schist extend far to the north and to the south of the belt, so that the total area of each is much greater than is shown in the table. The figures given for all the other bodies represent nearly their respective total areas. Less than 7 per cent of the belt is underlaid by rocks not clearly plutonic in origin, and of that 7 per cent perhaps half is greenstone or other igneous rock. The 3 or 4 per cent of non-igneous rock is chiefly concentrated in the tongues of Kruger s
. Bulletin of the Geological Society of America. Geology. RELATIONS OF BATITOLTTHIC AREAS 339 The batholxths and the Kruger schist extend far to the north and to the south of the belt, so that the total area of each is much greater than is shown in the table. The figures given for all the other bodies represent nearly their respective total areas. Less than 7 per cent of the belt is underlaid by rocks not clearly plutonic in origin, and of that 7 per cent perhaps half is greenstone or other igneous rock. The 3 or 4 per cent of non-igneous rock is chiefly concentrated in the tongues of Kruger schist. w e s T,E R N REMMEL. ,.-v v v Vâââ .-' V V V V V V "»,4 /' V V V V V V V v\ / vvvvvvvvv\ /vvvvvvvvvv*. ,'VVVVVVVVVVV *x .'vvvvvvvvvvvv\5\ PHASE OF /vvvvvvvvvvvvvv, fV V V V V' V V V V V V V V V Vk ⢠V VVVVVVVVVVV V V R A T H 0 L I T H-v v v vvvvvvvvvvvv on SVVVVVVVVVVVVVVV *,v v v v v v v v vvvvvvvv i V V V V V V V vvvvvvvv ^wPARK GRANITE â¢\ V V V V V V V V V VVVVVVVVV/ M iv V V V V /! V V V V V ,4- V v v _ .' +\v V V V .'" f fiV V V V/(V .â¢'+ + ; v v >+ + +v A + -f- + + + \ v v v v /â Â¥ + + + + + f V v v v + + + + + + + + \V V V t + HH + 4 +W â V V V V V V V V V V V V V V V V V V, V V V V W V V V V V V V V V V V V V V V ^vav basic v;*h;. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Geological Society of America. [New York : The Society]
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1890
